NOAA: U.S. Winter Temperatures For Every El NiƱo Since 1950

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U.S. Winter Temperature During Every El Nino Since 1950. Image: NOAA

NOAA:Ā U.S. Winter Temperatures For Every El NiƱo Since 1950

By:Ā Rebecca Lindsey

The tropical Pacific climate pattern known as “ENSO,” which is short for El NiƱo-Southern Oscillation, has its strongest influence on the U.S. climate during winter (December-February). El NiƱo in general acts to tilt the odds toward wetter- and cooler-than-average conditions across much of the South, and toward drier and warmer conditions in many of the northern regions. El NiƱo’sĀ influence on temperature is less reliable than its influence on precipitation.

The collection of maps at right show the difference from average (1981-2010) winter temperature (December-February) in each U.S. climate division during all El NiƱo events since 1950. Years are ranked from strongest El NiƱo (top left) to weakest (bottom right)ā€š based on the Decemberā€“FebruaryĀ Oceanic NiƱo IndexĀ value. There is no universal way to define the strength of El NiƱo events, but for this graphic, events with ONI values above 1.5 are ranked as strong, events with ONI values between 1 and 1.5 are ranked as moderate, and events with ONI values between 0.5 and 1 are ranked as weak.

These maps were first published on our ENSO blog as part of theĀ 2015-16 winter outlook postĀ by Mike Halpert, Deputy Director of NOAA’s Climate Prediction Center. They were updated for Halpert’sĀ post about the 2018-19 winter outlook.Ā In the original post, Halpert pointed out thatĀ compared to precipitation, temperature patterns are much less consistent, even during the strongest events.

Four of the six strong events have a warm signal that is nearly nationwide, but even among them, the geographic detailsā€”the location of the biggest anomalies, where the few cool spots areā€”vary from one event to another. Looking at both strong and moderate events, the patterns become even less consistent. Eight of the twelveĀ events have a warm signal in the Northern Plains (a much smaller area than is affected in the strong events), but 4 are colder than normal.

This variability from one ElĀ NiƱo to the next is one reason why CPC scientists always talk about seasonal climate outlooks in terms of “odds,” “chances,” or “probabilities”ā€”not guarantees. In the latest ENSO blog post,Ā Halpert explainsĀ how the weak ElĀ NiƱo predicted for the 2018-19 winter factors into NOAA’sĀ winter climate outlook, which favors warmer-than-normal temperatures across much of the country.


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